Weather Alert in North Carolina

Current Alerts for Tuckasegee, NC: Cold Weather Advisory High Wind Warning
Wind Advisory

Special Weather Statement issued February 6 at 3:01PM EST by NWS Greenville-Spartanburg SC

AREAS AFFECTED: Swain; Haywood; Graham

DESCRIPTION: Snow showers will develop across the high elevations of the Smokies this evening and then will continue through the early morning hours on Saturday, and finally tapering off by mid- morning. Elevations above 3500 feet right near the Tennessee border could get as much as 4-8 inches of snow by the time it ends, which would result in dangerous travel conditions on US Highway 441 across Newfound Gap. More populated areas of Graham, Swain, and Haywood counties may only get a dusting of snow, with maybe up to an inch around Balsam Gap and Soco Gap.

INSTRUCTION: N/A

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Weather Topic: What is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

Stratus Clouds Next Topic: Wall Clouds

Stratus clouds are similar to altostratus clouds, but form at a lower altitude and are identified by their fog-like appearance, lacking the distinguishing features of most clouds.

Stratus clouds are wider than most clouds, and their base has a smooth, uniform look which is lighter in color than a nimbostratus cloud. The presence of a stratus cloud indicates the possibility of minor precipitation, such as drizzle, but heavier precipitation does not typically arrive in the form of a stratus cloud.

Next Topic: Wall Clouds

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